Definition of the Subject
Brittle deformation is the primary mode of deformation of the Earth’s crust. At the long timescale it is manifested by faulting and on the short timescale by earthquakes. It is one of the best-known examples of a system exhibiting self-organized criticality. A full understanding of this system is essential to the evaluation of earthquake hazard.
Introduction
The upper part of the Earth’s crust is brittle and under a state of all-round compression. It responds to deformation by faulting: the formation and propagation of shear cracks. The crack walls support normal stresses, and hence fault propagation must overcome not only the rupture resistance of the fault tips but friction between its interior interfaces. This friction is usually velocity weakening, such that any slippage results in stick–slip instability. The resulting dynamically running crack-like shear instability radiates elastic waves, producing the shaking known as an earthquake. Thus brittle...
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Abbreviations
- Ductile shear zone:
-
A quasi-planar tabular zone of localized shear deformation in the semi-brittle to fully plastic regimes.
- Earthquake:
-
Dynamically running shear instability on a fault.
- Fault:
-
A shear crack with friction between its interfaces.
- Mylonite:
-
A metamorphic rock with a fabric produced by shear deformation.
- Suprafault:
-
The shear relaxation structure that includes a fault and its associated ductile shear zone.
Bibliography
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Books and Reviews
Sornette D (2003) Critical phenomena in natural systems: Chaos, fractals, self-organization, and disorder. Springer, Berlin
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Scholz, C.H. (2014). Brittle Tectonics: A Nonlinear Dynamic System. In: Meyers, R. (eds) Encyclopedia of Complexity and Systems Science. Springer, New York, NY. https://doi.org/10.1007/978-3-642-27737-5_44-2
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DOI: https://doi.org/10.1007/978-3-642-27737-5_44-2
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